Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula
- Autores
- Daura, J.; Sanz, M.; Julià, R.; García Fernández, D.; Fornós, Joan J.; Vaquero, M.; Allué, E.; López García, J. M.; Blain. H. A.; Ortiz, J. E.; Torres, T.; Albert, R. M.; Rodríguez Cintas, A.; Sánchez Marco, Antonio; Cerdeño Serrano, Maria Esperanza; Skinner, A. R.; Asmeron, Y.; Polyak, V. J.; Garcés, M.; Arnold, L. J.; Demuro, M.; Pike, A. W. G.; Euba, I.; Rodríguez, R. F.; Yagüe, A. S.; Villaescusa, L.; Gómez, S.; Rubio, A.; Pedro, M.; Fullola, J. M.; Zilhão, João
- Año de publicación
- 2015
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Cova del Rinoceront, a site in NE Iberia, contains a thick sedimentary fill preserving a faunal archive from the penultimate glacial and the the last interglacial periods. Layers I to III have been dated to between 74 and 147ka, coinciding with MIS 5a to 5e, a period poorly represented in the Mediterranean terrestrial record. The results from Cova del Rinoceront are of broader interest for the reconstruction of ecological dynamics during warm stages and the understanding of the evolution and geographical variation of several taxa. The palaeoecological evidence suggests a landscape dominated by mixed wooded vegetation with mild climatic conditions, slightly more humid than today. Several vertebrate taxa, including Haploidoceros mediterraneus, Stephanorhinus hundsheimensis and Glis glis, are documented for the first time in the early Upper Pleistocene of Europe, showing that these species persisted across the region for longer than previously thought. In addition, the recovery of a small lithic assemblage indicates human presence in the surroundings of the site. The 11m-thick stratigraphic section also provides an ideal setting in which to compare several geochronological methods. U-Th dating of the flowstones that cap the deposit, of speleothems formed along the cave walls, and of speleothems buried by the deposit at different elevations provides minimum and maximum ages of 74 and 175ka, respectively, for the accumulation. The ages obtained by luminescence, electron spin resonance (ESR), amino acid racemisation (AAR), palaeomagnetism and U-series dating of bone are in good agreement with each other and are stratigraphically consistent. This well-dated faunal succession presents a unique opportunity to assess changes in the Pleistocene fauna of the Mediterranean coast over an interval of more than 100ka.
Fil: Daura, J.. Universidad de Barcelona; España
Fil: Sanz, M.. Universidad de Barcelona; España
Fil: Julià, R.. Consejo Superior de Investigaciones Científicas. Instituto de Ciencias de la Tierra Jaume Almera; España
Fil: García Fernández, D.. Universidad de Barcelona; España
Fil: Fornós, Joan J.. Universidad de las Islas Baleares; España
Fil: Vaquero, M.. Universitat Rovira i Virgili. Institut Català de Paleoecologia Humana i Evolució Social; España
Fil: Allué, E.. Universitat Rovira i Virgili. Institut Català de Paleoecologia Humana i Evolució Social; España
Fil: López García, J. M.. Università di Ferrara; Italia
Fil: Blain. H. A.. Universitat Rovira i Virgili. Institut Català de Paleoecologia Humana i Evolució Social; España
Fil: Ortiz, J. E.. Universidad Politécnica de Madrid; España
Fil: Torres, T.. Universidad Politécnica de Madrid; España
Fil: Albert, R. M.. Universidad de Barcelona; España. Institució Catalana de Recerca i Estudis Avancats; España
Fil: Rodríguez Cintas, A.. Universidad de Barcelona; España
Fil: Sánchez Marco, Antonio. Universitat Autònoma de Barcelona; España
Fil: Cerdeño Serrano, Maria Esperanza. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Skinner, A. R.. Williams College; Estados Unidos
Fil: Asmeron, Y.. University of New Mexico; Estados Unidos
Fil: Polyak, V. J.. University of New Mexico; Estados Unidos
Fil: Garcés, M.. Universidad de Barcelona; España
Fil: Arnold, L. J.. University of Adelaide; Australia
Fil: Demuro, M.. University of Adelaide; Australia
Fil: Pike, A. W. G.. University of Southampton; Reino Unido
Fil: Euba, I.. Institut Català d'Arqueologia Clàssica; España
Fil: Rodríguez, R. F.. Universidad de Barcelona; España
Fil: Yagüe, A. S.. Universidad de Barcelona; España
Fil: Villaescusa, L.. Universidad de Barcelona; España
Fil: Gómez, S.. Universidad de Barcelona; España
Fil: Rubio, A.. Universidad de Barcelona; España. Universidad de Granada; España
Fil: Pedro, M.. Universidad de Barcelona; España
Fil: Fullola, J. M.. Universidad de Barcelona; España
Fil: Zilhão, João. Universidad de Barcelona; España. Institució Catalana de Recerca i Estudis Avancats; España - Materia
-
Cova del Rinoceront
Iberian Peninsula
Mis 5
Multiproxy Data
Palaeoenvironment
Upper Pleistocene - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/50112
Ver los metadatos del registro completo
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Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian PeninsulaDaura, J.Sanz, M.Julià, R.García Fernández, D.Fornós, Joan J.Vaquero, M.Allué, E.López García, J. M.Blain. H. A.Ortiz, J. E.Torres, T.Albert, R. M.Rodríguez Cintas, A.Sánchez Marco, AntonioCerdeño Serrano, Maria EsperanzaSkinner, A. R.Asmeron, Y.Polyak, V. J.Garcés, M.Arnold, L. J.Demuro, M.Pike, A. W. G.Euba, I.Rodríguez, R. F.Yagüe, A. S.Villaescusa, L.Gómez, S.Rubio, A.Pedro, M.Fullola, J. M.Zilhão, JoãoCova del RinocerontIberian PeninsulaMis 5Multiproxy DataPalaeoenvironmentUpper Pleistocenehttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Cova del Rinoceront, a site in NE Iberia, contains a thick sedimentary fill preserving a faunal archive from the penultimate glacial and the the last interglacial periods. Layers I to III have been dated to between 74 and 147ka, coinciding with MIS 5a to 5e, a period poorly represented in the Mediterranean terrestrial record. The results from Cova del Rinoceront are of broader interest for the reconstruction of ecological dynamics during warm stages and the understanding of the evolution and geographical variation of several taxa. The palaeoecological evidence suggests a landscape dominated by mixed wooded vegetation with mild climatic conditions, slightly more humid than today. Several vertebrate taxa, including Haploidoceros mediterraneus, Stephanorhinus hundsheimensis and Glis glis, are documented for the first time in the early Upper Pleistocene of Europe, showing that these species persisted across the region for longer than previously thought. In addition, the recovery of a small lithic assemblage indicates human presence in the surroundings of the site. The 11m-thick stratigraphic section also provides an ideal setting in which to compare several geochronological methods. U-Th dating of the flowstones that cap the deposit, of speleothems formed along the cave walls, and of speleothems buried by the deposit at different elevations provides minimum and maximum ages of 74 and 175ka, respectively, for the accumulation. The ages obtained by luminescence, electron spin resonance (ESR), amino acid racemisation (AAR), palaeomagnetism and U-series dating of bone are in good agreement with each other and are stratigraphically consistent. This well-dated faunal succession presents a unique opportunity to assess changes in the Pleistocene fauna of the Mediterranean coast over an interval of more than 100ka.Fil: Daura, J.. Universidad de Barcelona; EspañaFil: Sanz, M.. Universidad de Barcelona; EspañaFil: Julià, R.. Consejo Superior de Investigaciones Científicas. Instituto de Ciencias de la Tierra Jaume Almera; EspañaFil: García Fernández, D.. Universidad de Barcelona; EspañaFil: Fornós, Joan J.. Universidad de las Islas Baleares; EspañaFil: Vaquero, M.. Universitat Rovira i Virgili. Institut Català de Paleoecologia Humana i Evolució Social; EspañaFil: Allué, E.. Universitat Rovira i Virgili. Institut Català de Paleoecologia Humana i Evolució Social; EspañaFil: López García, J. M.. Università di Ferrara; ItaliaFil: Blain. H. A.. Universitat Rovira i Virgili. Institut Català de Paleoecologia Humana i Evolució Social; EspañaFil: Ortiz, J. E.. Universidad Politécnica de Madrid; EspañaFil: Torres, T.. Universidad Politécnica de Madrid; EspañaFil: Albert, R. M.. Universidad de Barcelona; España. Institució Catalana de Recerca i Estudis Avancats; EspañaFil: Rodríguez Cintas, A.. Universidad de Barcelona; EspañaFil: Sánchez Marco, Antonio. Universitat Autònoma de Barcelona; EspañaFil: Cerdeño Serrano, Maria Esperanza. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Skinner, A. R.. Williams College; Estados UnidosFil: Asmeron, Y.. University of New Mexico; Estados UnidosFil: Polyak, V. J.. University of New Mexico; Estados UnidosFil: Garcés, M.. Universidad de Barcelona; EspañaFil: Arnold, L. J.. University of Adelaide; AustraliaFil: Demuro, M.. University of Adelaide; AustraliaFil: Pike, A. W. G.. University of Southampton; Reino UnidoFil: Euba, I.. Institut Català d'Arqueologia Clàssica; EspañaFil: Rodríguez, R. F.. Universidad de Barcelona; EspañaFil: Yagüe, A. S.. Universidad de Barcelona; EspañaFil: Villaescusa, L.. Universidad de Barcelona; EspañaFil: Gómez, S.. Universidad de Barcelona; EspañaFil: Rubio, A.. Universidad de Barcelona; España. Universidad de Granada; EspañaFil: Pedro, M.. Universidad de Barcelona; EspañaFil: Fullola, J. M.. Universidad de Barcelona; EspañaFil: Zilhão, João. Universidad de Barcelona; España. Institució Catalana de Recerca i Estudis Avancats; EspañaPergamon-Elsevier Science Ltd2015-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/50112Daura, J.; Sanz, M.; Julià, R.; García Fernández, D.; Fornós, Joan J.; et al.; Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula; Pergamon-Elsevier Science Ltd; Quaternary Science Reviews; 114; 4-2015; 203-2270277-3791CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0277379115000761info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2015.02.014info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:08:22Zoai:ri.conicet.gov.ar:11336/50112instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 10:08:22.792CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula |
| title |
Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula |
| spellingShingle |
Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula Daura, J. Cova del Rinoceront Iberian Peninsula Mis 5 Multiproxy Data Palaeoenvironment Upper Pleistocene |
| title_short |
Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula |
| title_full |
Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula |
| title_fullStr |
Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula |
| title_full_unstemmed |
Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula |
| title_sort |
Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula |
| dc.creator.none.fl_str_mv |
Daura, J. Sanz, M. Julià, R. García Fernández, D. Fornós, Joan J. Vaquero, M. Allué, E. López García, J. M. Blain. H. A. Ortiz, J. E. Torres, T. Albert, R. M. Rodríguez Cintas, A. Sánchez Marco, Antonio Cerdeño Serrano, Maria Esperanza Skinner, A. R. Asmeron, Y. Polyak, V. J. Garcés, M. Arnold, L. J. Demuro, M. Pike, A. W. G. Euba, I. Rodríguez, R. F. Yagüe, A. S. Villaescusa, L. Gómez, S. Rubio, A. Pedro, M. Fullola, J. M. Zilhão, João |
| author |
Daura, J. |
| author_facet |
Daura, J. Sanz, M. Julià, R. García Fernández, D. Fornós, Joan J. Vaquero, M. Allué, E. López García, J. M. Blain. H. A. Ortiz, J. E. Torres, T. Albert, R. M. Rodríguez Cintas, A. Sánchez Marco, Antonio Cerdeño Serrano, Maria Esperanza Skinner, A. R. Asmeron, Y. Polyak, V. J. Garcés, M. Arnold, L. J. Demuro, M. Pike, A. W. G. Euba, I. Rodríguez, R. F. Yagüe, A. S. Villaescusa, L. Gómez, S. Rubio, A. Pedro, M. Fullola, J. M. Zilhão, João |
| author_role |
author |
| author2 |
Sanz, M. Julià, R. García Fernández, D. Fornós, Joan J. Vaquero, M. Allué, E. López García, J. M. Blain. H. A. Ortiz, J. E. Torres, T. Albert, R. M. Rodríguez Cintas, A. Sánchez Marco, Antonio Cerdeño Serrano, Maria Esperanza Skinner, A. R. Asmeron, Y. Polyak, V. J. Garcés, M. Arnold, L. J. Demuro, M. Pike, A. W. G. Euba, I. Rodríguez, R. F. Yagüe, A. S. Villaescusa, L. Gómez, S. Rubio, A. Pedro, M. Fullola, J. M. Zilhão, João |
| author2_role |
author author author author author author author author author author author author author author author author author author author author author author author author author author author author author author |
| dc.subject.none.fl_str_mv |
Cova del Rinoceront Iberian Peninsula Mis 5 Multiproxy Data Palaeoenvironment Upper Pleistocene |
| topic |
Cova del Rinoceront Iberian Peninsula Mis 5 Multiproxy Data Palaeoenvironment Upper Pleistocene |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
The Cova del Rinoceront, a site in NE Iberia, contains a thick sedimentary fill preserving a faunal archive from the penultimate glacial and the the last interglacial periods. Layers I to III have been dated to between 74 and 147ka, coinciding with MIS 5a to 5e, a period poorly represented in the Mediterranean terrestrial record. The results from Cova del Rinoceront are of broader interest for the reconstruction of ecological dynamics during warm stages and the understanding of the evolution and geographical variation of several taxa. The palaeoecological evidence suggests a landscape dominated by mixed wooded vegetation with mild climatic conditions, slightly more humid than today. Several vertebrate taxa, including Haploidoceros mediterraneus, Stephanorhinus hundsheimensis and Glis glis, are documented for the first time in the early Upper Pleistocene of Europe, showing that these species persisted across the region for longer than previously thought. In addition, the recovery of a small lithic assemblage indicates human presence in the surroundings of the site. The 11m-thick stratigraphic section also provides an ideal setting in which to compare several geochronological methods. U-Th dating of the flowstones that cap the deposit, of speleothems formed along the cave walls, and of speleothems buried by the deposit at different elevations provides minimum and maximum ages of 74 and 175ka, respectively, for the accumulation. The ages obtained by luminescence, electron spin resonance (ESR), amino acid racemisation (AAR), palaeomagnetism and U-series dating of bone are in good agreement with each other and are stratigraphically consistent. This well-dated faunal succession presents a unique opportunity to assess changes in the Pleistocene fauna of the Mediterranean coast over an interval of more than 100ka. Fil: Daura, J.. Universidad de Barcelona; España Fil: Sanz, M.. Universidad de Barcelona; España Fil: Julià, R.. Consejo Superior de Investigaciones Científicas. Instituto de Ciencias de la Tierra Jaume Almera; España Fil: García Fernández, D.. Universidad de Barcelona; España Fil: Fornós, Joan J.. Universidad de las Islas Baleares; España Fil: Vaquero, M.. Universitat Rovira i Virgili. Institut Català de Paleoecologia Humana i Evolució Social; España Fil: Allué, E.. Universitat Rovira i Virgili. Institut Català de Paleoecologia Humana i Evolució Social; España Fil: López García, J. M.. Università di Ferrara; Italia Fil: Blain. H. A.. Universitat Rovira i Virgili. Institut Català de Paleoecologia Humana i Evolució Social; España Fil: Ortiz, J. E.. Universidad Politécnica de Madrid; España Fil: Torres, T.. Universidad Politécnica de Madrid; España Fil: Albert, R. M.. Universidad de Barcelona; España. Institució Catalana de Recerca i Estudis Avancats; España Fil: Rodríguez Cintas, A.. Universidad de Barcelona; España Fil: Sánchez Marco, Antonio. Universitat Autònoma de Barcelona; España Fil: Cerdeño Serrano, Maria Esperanza. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina Fil: Skinner, A. R.. Williams College; Estados Unidos Fil: Asmeron, Y.. University of New Mexico; Estados Unidos Fil: Polyak, V. J.. University of New Mexico; Estados Unidos Fil: Garcés, M.. Universidad de Barcelona; España Fil: Arnold, L. J.. University of Adelaide; Australia Fil: Demuro, M.. University of Adelaide; Australia Fil: Pike, A. W. G.. University of Southampton; Reino Unido Fil: Euba, I.. Institut Català d'Arqueologia Clàssica; España Fil: Rodríguez, R. F.. Universidad de Barcelona; España Fil: Yagüe, A. S.. Universidad de Barcelona; España Fil: Villaescusa, L.. Universidad de Barcelona; España Fil: Gómez, S.. Universidad de Barcelona; España Fil: Rubio, A.. Universidad de Barcelona; España. Universidad de Granada; España Fil: Pedro, M.. Universidad de Barcelona; España Fil: Fullola, J. M.. Universidad de Barcelona; España Fil: Zilhão, João. Universidad de Barcelona; España. Institució Catalana de Recerca i Estudis Avancats; España |
| description |
The Cova del Rinoceront, a site in NE Iberia, contains a thick sedimentary fill preserving a faunal archive from the penultimate glacial and the the last interglacial periods. Layers I to III have been dated to between 74 and 147ka, coinciding with MIS 5a to 5e, a period poorly represented in the Mediterranean terrestrial record. The results from Cova del Rinoceront are of broader interest for the reconstruction of ecological dynamics during warm stages and the understanding of the evolution and geographical variation of several taxa. The palaeoecological evidence suggests a landscape dominated by mixed wooded vegetation with mild climatic conditions, slightly more humid than today. Several vertebrate taxa, including Haploidoceros mediterraneus, Stephanorhinus hundsheimensis and Glis glis, are documented for the first time in the early Upper Pleistocene of Europe, showing that these species persisted across the region for longer than previously thought. In addition, the recovery of a small lithic assemblage indicates human presence in the surroundings of the site. The 11m-thick stratigraphic section also provides an ideal setting in which to compare several geochronological methods. U-Th dating of the flowstones that cap the deposit, of speleothems formed along the cave walls, and of speleothems buried by the deposit at different elevations provides minimum and maximum ages of 74 and 175ka, respectively, for the accumulation. The ages obtained by luminescence, electron spin resonance (ESR), amino acid racemisation (AAR), palaeomagnetism and U-series dating of bone are in good agreement with each other and are stratigraphically consistent. This well-dated faunal succession presents a unique opportunity to assess changes in the Pleistocene fauna of the Mediterranean coast over an interval of more than 100ka. |
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2015 |
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2015-04 |
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http://hdl.handle.net/11336/50112 Daura, J.; Sanz, M.; Julià, R.; García Fernández, D.; Fornós, Joan J.; et al.; Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula; Pergamon-Elsevier Science Ltd; Quaternary Science Reviews; 114; 4-2015; 203-227 0277-3791 CONICET Digital CONICET |
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Daura, J.; Sanz, M.; Julià, R.; García Fernández, D.; Fornós, Joan J.; et al.; Cova del Rinoceront (Castelldefels, Barcelona): a terrestrial record for the Last Interglacial period (MIS 5) in the Mediterranean coast of the Iberian Peninsula; Pergamon-Elsevier Science Ltd; Quaternary Science Reviews; 114; 4-2015; 203-227 0277-3791 CONICET Digital CONICET |
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eng |
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eng |
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Pergamon-Elsevier Science Ltd |
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